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,{"id":35294,"text":"b1068 - 1959 - Geology of Wabaunsee County, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"b1068","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1068","title":"Geology of Wabaunsee County, Kansas","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1068","usgsCitation":"Mudge, M.R., and Burton, R.H., 1959, Geology of Wabaunsee County, Kansas: U.S. Geological Survey Bulletin 1068, 210 p. ill., maps (1 col.) ;23 cm., https://doi.org/10.3133/b1068.","productDescription":"210 p. ill., maps (1 col.) ;23 cm.","costCenters":[],"links":[{"id":109270,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20706.htm","linkFileType":{"id":5,"text":"html"},"description":"20706"},{"id":96877,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-16.pdf","size":"102","linkFileType":{"id":1,"text":"pdf"}},{"id":96878,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-18.pdf","size":"413","linkFileType":{"id":1,"text":"pdf"}},{"id":96879,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-table_1.pdf","size":"833","linkFileType":{"id":1,"text":"pdf"}},{"id":96865,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1068/report.pdf","size":"17294","linkFileType":{"id":1,"text":"pdf"}},{"id":96866,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-01.pdf","size":"545","linkFileType":{"id":1,"text":"pdf"}},{"id":96867,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-02.pdf","size":"11099","linkFileType":{"id":1,"text":"pdf"}},{"id":96868,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-03.pdf","size":"1295","linkFileType":{"id":1,"text":"pdf"}},{"id":96869,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-04.pdf","size":"795","linkFileType":{"id":1,"text":"pdf"}},{"id":96870,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-07.pdf","size":"308","linkFileType":{"id":1,"text":"pdf"}},{"id":96871,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-08.pdf","size":"365","linkFileType":{"id":1,"text":"pdf"}},{"id":96872,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-09.pdf","size":"196","linkFileType":{"id":1,"text":"pdf"}},{"id":96873,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-10.pdf","size":"530","linkFileType":{"id":1,"text":"pdf"}},{"id":96874,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-11.pdf","size":"811","linkFileType":{"id":1,"text":"pdf"}},{"id":96875,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-13.pdf","size":"683","linkFileType":{"id":1,"text":"pdf"}},{"id":96876,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1068/plate-14.pdf","size":"900","linkFileType":{"id":1,"text":"pdf"}},{"id":167277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1068/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683746","contributors":{"authors":[{"text":"Mudge, Melville Rhodes","contributorId":77119,"corporation":false,"usgs":true,"family":"Mudge","given":"Melville","email":"","middleInitial":"Rhodes","affiliations":[],"preferred":false,"id":214401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burton, Robert H.","contributorId":15630,"corporation":false,"usgs":true,"family":"Burton","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214400,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":39140,"text":"pp280K - 1959 - Part 4. Submarine topography and shoal-water ecology","interactions":[],"lastModifiedDate":"2022-02-17T22:43:58.618476","indexId":"pp280K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"280","chapter":"K","title":"Part 4. Submarine topography and shoal-water ecology","docAbstract":"<p>The topography of the sea floor within 10 miles of Saipan broadly resembles that of the land. Eastward, toward the Mariana trench, slopes are about 6&deg;, without prominent benches or scarps. This is inferred to indicate easterly continuation of generally pyroclastic bedrock. The westward slope averages 2&deg; to 3&deg; and consists mainly of nearly flat benches and westfacing scarps. This is taken to imply westward continuation of a limestone bench-and-fault-scarp topography. Projection of known faults to sea and through Tinian, on the basis of topographic trends, suggests a pattern of west-dipping normal faults that parallel the strike of the Mariana ridge and affect the shape and position of islands at the crest of the ridge.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology of Saipan, Mariana Islands","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp280K","usgsCitation":"Cloud, P.E., 1959, Part 4. Submarine topography and shoal-water ecology: U.S. Geological Survey Professional Paper 280, Report: 134 p.; 4 Plates: 27.31 x 35.94 inches or smaller; Table 6; Chart 1, https://doi.org/10.3133/pp280K.","productDescription":"Report: 134 p.; 4 Plates: 27.31 x 35.94 inches or smaller; Table 6; Chart 1","startPage":"361","endPage":"445","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":122170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0280k/report-thumb.jpg"},{"id":66639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0280k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":321976,"rank":306,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/pp/0280k/table-6.pdf","text":"Table 6","linkFileType":{"id":1,"text":"pdf"}},{"id":321975,"rank":305,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0280k/plate-122.pdf","text":"Plate 122","linkFileType":{"id":1,"text":"pdf"}},{"id":321974,"rank":304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0280k/plate-121.pdf","text":"Plate 121","linkFileType":{"id":1,"text":"pdf"}},{"id":321973,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0280k/plate-120.pdf","text":"Plate 120","linkFileType":{"id":1,"text":"pdf"}},{"id":321972,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0280k/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":321971,"rank":301,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/0280k/chart-1.pdf","text":"Chart 1","linkFileType":{"id":1,"text":"pdf"}},{"id":396148,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_44665.htm"}],"country":"Saipan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              145.6835174560547,\n              15.088698509791715\n            ],\n            [\n              145.6835174560547,\n              15.295444914728776\n            ],\n            [\n              145.83457946777344,\n              15.295444914728776\n            ],\n            [\n              145.83457946777344,\n              15.088698509791715\n            ],\n            [\n              145.6835174560547,\n              15.088698509791715\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683ba0","contributors":{"authors":[{"text":"Cloud, Preston E. Jr.","contributorId":59861,"corporation":false,"usgs":true,"family":"Cloud","given":"Preston","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":221028,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":686,"text":"wsp1448 - 1959 - Surface water supply of the United States, 1956, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1448","title":"Surface water supply of the United States, 1956, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1448","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1959, Surface water supply of the United States, 1956, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1448, viii, 305 p. ;23 cm., https://doi.org/10.3133/wsp1448.","productDescription":"viii, 305 p. ;23 cm.","costCenters":[],"links":[{"id":137318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1448/report-thumb.jpg"},{"id":25249,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69613d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64345,"text":"gp200 - 1959 - Aeromagnetic map of the Valley Forge quadrangle, Chester, Montgomery, and Delaware Counties, Pennsylvania","interactions":[],"lastModifiedDate":"2025-04-04T18:58:05.266505","indexId":"gp200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"200","title":"Aeromagnetic map of the Valley Forge quadrangle, Chester, Montgomery, and Delaware Counties, Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp200","usgsCitation":"Bromery, R.W., and Zandle, G.L., 1959, Aeromagnetic map of the Valley Forge quadrangle, Chester, Montgomery, and Delaware Counties, Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 200, 1 Plate: 22.91 x 26.76 inches, https://doi.org/10.3133/gp200.","productDescription":"1 Plate: 22.91 x 26.76 inches","costCenters":[],"links":[{"id":251733,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0200/report-thumb.jpg"},{"id":251004,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0200/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251003,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0200/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":484211,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3119.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Pennsylvania","county":"Chester County, Delaware County, Montgomery County","otherGeospatial":"Valley Forge quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.5,40 ], [ -75.5,40.1175 ], [ -75.375,40.1175 ], [ -75.375,40 ], [ -75.5,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c0ff","contributors":{"authors":[{"text":"Bromery, Randolph Wilson","contributorId":22746,"corporation":false,"usgs":true,"family":"Bromery","given":"Randolph","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":270652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270653,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2564,"text":"wsp1472 - 1959 - Hydrologic budget of the Beaverdam Creek basin, Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp1472","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1472","title":"Hydrologic budget of the Beaverdam Creek basin, Maryland","docAbstract":"A hydrologic budget is a statement accounting for the water gains and losses for selected periods in an area. Weekly measurements of precipitation streamflow, surface-water storage, ground-water stage, and soil resistivity were made during a 2year period, April 1, 1950, to March 28, 1952, in the Beaverdam Creek basin, Wicomico County, Md. The hydrologic measurements are summarized in two budgets, a total budget and a ground-water budget, and in supporting tables and graphs. \r\n\r\nThe results of the investigation have some potentially significant applications because they describe a method for determining the annual replenishment of the water supply of a basin and the ways of water disposal under natural conditions. The information helps to determine the 'safe' yield of water in diversion from natural to artificial discharge. The drainage basin of Beaverdam Creek was selected because it appeared to have fewer hydrologic variables than are generally found. However, the methods may prove applicable in many places under a variety of conditions. \r\n\r\nThe measurements are expressed in inches of water over the area of the basin. The equation of the hydrologic cycle is the budget balance: P= R+E+ASW+ delta SW + delta SM + delta GW where P is precipitation; R is runoff; ET is evapotranspiration; delta SW is change in surface-water storage; delta SM is change in soil moisture; and delta GW is change in ground-water storage. In this report 'change' is the final quantity minus the initial quantity and thus is synonymous with 'increase.' Further, ,delta GW= delta H .x Yg, \r\n\r\nin which delta H is the change in ground-water stage and Yg is the gravity yield, or the specific yield of the sediments as measured during the short periods of declining ground-water levels characteristic of the area. The complex sum of the revised equation P ? R - delta SW ? ET - delta SM, which is equal to delta H. x Yg, has been named the \r\n\r\n'infiltration residual'; it is equivalent to ground-water recharge. Two unmeasured, but not entirely unknown, quantities, evapotranspiration, (ET) and gravity yield, (Yg), are included in the equation. They are derived statistically by a method of convergent approximations, one of the contributions of this investigation. \r\n\r\nOn the basis of laboratory analysis, well-field tests, and general information on rates of drainage from saturated sediments, a gravity yield of 14 percent was assumed as a first approximation. The equation was then solved, by weeks, for evapotranspiration, ET. The evapotranspiration losses were plotted against the calendar week. Using the time of year as a control, a smooth curve was fitted to the evapotranspiration data, and modified values of ET were read from the curve. These were used to compute weekly values of the infiltration residual which were plotted against ground-water stage. The slope of the line of best fit gave a closer approximation of gravity yield, Yg. The process was repeated. The approximations converged, so that a fourth and final approximation resulted in a close grouping of all the points along a line whose slope indicated a Yg of 11.0 percent, and a slightly asymmetric bell-shaped curve of total evapotranspiration by weeks was obtained that is considered representative of this area. Check calculations of gravity yield were made during periods of low evapotranspiration and high infiltration, which substantiate the computed average of 11.0 percent. \r\n\r\nRefinements in the method of deriving the ground-water budget were introduced to supplement the techniques developed by Meinzer and Stearns in the study of the Pomperaug River basin in Connecticut in 1913 and 1916. The hydrologic equation for the ground-water cycle may be written Gr=D + delta H. x Yg + ETg, in which Gr is ground-water recharge (infiltration); D is ground-water drainage; delta H is the change in mean ground-water stage (final stage minus initial stage); Yg is gravity yield (taken as 11.0 percent in computations here); an","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1472","usgsCitation":"Rasmussen, W.C., and Andreasen, G., 1959, Hydrologic budget of the Beaverdam Creek basin, Maryland: U.S. Geological Survey Water Supply Paper 1472, v, 106 p., [2] leaves of plates :ill., maps ;25 cm., https://doi.org/10.3133/wsp1472.","productDescription":"v, 106 p., [2] leaves of plates :ill., maps ;25 cm.","costCenters":[],"links":[{"id":138583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1472/report-thumb.jpg"},{"id":247225,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1472/plate-05.pdf","size":"561","linkFileType":{"id":1,"text":"pdf"}},{"id":247226,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1472/plate-06.pdf","size":"502","linkFileType":{"id":1,"text":"pdf"}},{"id":247227,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1472/plate-07.pdf","size":"1090","linkFileType":{"id":1,"text":"pdf"}},{"id":247228,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1472/plate-10.pdf","size":"424","linkFileType":{"id":1,"text":"pdf"}},{"id":247222,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1472/plate-01.pdf","size":"1134","linkFileType":{"id":1,"text":"pdf"}},{"id":247223,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1472/plate-03.pdf","size":"576","linkFileType":{"id":1,"text":"pdf"}},{"id":247224,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1472/plate-04.pdf","size":"749","linkFileType":{"id":1,"text":"pdf"}},{"id":28830,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1472/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611692","contributors":{"authors":[{"text":"Rasmussen, W. C.","contributorId":62201,"corporation":false,"usgs":true,"family":"Rasmussen","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145405,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, Gordon E.","contributorId":94272,"corporation":false,"usgs":true,"family":"Andreasen","given":"Gordon E.","affiliations":[],"preferred":false,"id":145406,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3954,"text":"cir419 - 1959 - The definition of known geologic structures of producing oil and gas fields","interactions":[],"lastModifiedDate":"2017-06-17T13:13:18","indexId":"cir419","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"419","title":"The definition of known geologic structures of producing oil and gas fields","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir419","usgsCitation":"Finley, E.A., 1959, The definition of known geologic structures of producing oil and gas fields: U.S. Geological Survey Circular 419, 6 p. :ill. ;26 cm., https://doi.org/10.3133/cir419.","productDescription":"6 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":31041,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1959/0419/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1959/0419/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ebd","contributors":{"authors":[{"text":"Finley, Emmett A.","contributorId":47348,"corporation":false,"usgs":true,"family":"Finley","given":"Emmett","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147889,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1326,"text":"wsp1470 - 1959 - Geology and ground-water features of the Eureka area, Humboldt County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1470","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1470","title":"Geology and ground-water features of the Eureka area, Humboldt County, California","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1470","usgsCitation":"Evenson, R.E., 1959, Geology and ground-water features of the Eureka area, Humboldt County, California: U.S. Geological Survey Water Supply Paper 1470, iv, 80 p. :maps, diagrs., tables. ;25 cm., https://doi.org/10.3133/wsp1470.","productDescription":"iv, 80 p. :maps, diagrs., tables. ;25 cm.","costCenters":[],"links":[{"id":137989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1470/report-thumb.jpg"},{"id":26375,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1470/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26376,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1470/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1470/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f75","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143568,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1844,"text":"wsp1459A - 1959 - Survey of ferrous-ferric chemical equilibria and redox potentials","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1459A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1459","chapter":"A","title":"Survey of ferrous-ferric chemical equilibria and redox potentials","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1459A","usgsCitation":"Hem, J.D., and Cropper, W., 1959, Survey of ferrous-ferric chemical equilibria and redox potentials: U.S. Geological Survey Water Supply Paper 1459, iii, 31 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1459A.","productDescription":"iii, 31 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1459a/report-thumb.jpg"},{"id":27050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1459a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688869","contributors":{"authors":[{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":144241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cropper, W.H.","contributorId":93029,"corporation":false,"usgs":true,"family":"Cropper","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":144242,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61493,"text":"mf212 - 1959 - Preliminary geologic and structure map of the southeast part of the Cascade Springs quadrangle, Fall River County, South Dakota","interactions":[],"lastModifiedDate":"2018-12-14T11:09:00","indexId":"mf212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"212","title":"Preliminary geologic and structure map of the southeast part of the Cascade Springs quadrangle, Fall River County, South Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf212","usgsCitation":"Post, E., 1959, Preliminary geologic and structure map of the southeast part of the Cascade Springs quadrangle, Fall River County, South Dakota: U.S. Geological Survey Miscellaneous Field Studies Map 212, 36.56 x 30.57 inches, https://doi.org/10.3133/mf212.","productDescription":"36.56 x 30.57 inches","costCenters":[],"links":[{"id":360300,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0212/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":187303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0212/report-thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Fall River County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.55111111111111,43.25 ], [ -103.55111111111111,43.284166666666664 ], [ -103.5,43.284166666666664 ], [ -103.5,43.25 ], [ -103.55111111111111,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c2f4","contributors":{"authors":[{"text":"Post, Edwin V.","contributorId":80330,"corporation":false,"usgs":true,"family":"Post","given":"Edwin V.","affiliations":[],"preferred":false,"id":265809,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1035,"text":"wsp1483 - 1959 - Geology and ground-water resources of the upper Lodgepole Creek drainage basin, Wyoming, with a section on chemical quality of the water","interactions":[],"lastModifiedDate":"2017-09-20T16:00:17","indexId":"wsp1483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1483","title":"Geology and ground-water resources of the upper Lodgepole Creek drainage basin, Wyoming, with a section on chemical quality of the water","docAbstract":"The principal sources of ground-water supply in the upper Lodgepole Creek drainage basin-the part of the basin west of the Wyoming-Nebraska State line-are the Brule formation of Oligocene age, the Arikaree formation of Miocene age, the Ogallala formation of Pliocene age, and the unconsolidated deposits of Quaternary age. \r\n\r\nThe Brule formation is a moderately hard siltstone that generally is not a good aquifer. However, where it is fractured or where the upper part consists of pebbles of reworked siltstone, it will yield large quantities of water to wells. Many wells in the Pine Bluffs lowland, at the east end of the area, derive water from the Brule. The Arikaree formation, which consists of loosely to moderately cemented fine sand, will yield small quantities of water to wells but is not thick enough or permeable enough to supply sufficient water for irrigation. Only a few wells derive water from it. The Ogallala formation consists of lenticular beds of clay, silt, sand, and gravel which, in part, are cemented with calcium carbonate. Only the lower part of the formation is saturated. Nearly all the wells in the upland part of the area tap the Ogallala, but they supply water in amounts sufficient for domestic and stock use only. Two of the wells have a moderately large discharge, and other wells of comparable discharge probably could be drilled in those parts of the upland where the saturated part of the Ogallala is fairly thick. Most of the unconsolidated deposits of Quaternary age are very permeable and, where a sufficient thickness is saturated, will yield large quantities of water to wells. These deposits are a significant source of water supply in the southeastern part of the area. \r\n\r\nThe Chadron formation of Oligocene age, which underlies the Brule formation, is a medium- to coarse-grained sandstone where it crops out in the Islay lowland. No wells tap the Chadron, but it probably would yield small quantities of water to wells. It lies at a relatively shallow depth beneath most of the Islay lowland, near the west end of the area, and at a depth of about 800 feet beneath the Pine Bluffs lowland. In the latter area it probably is finer grained and may not be permeable enough to yield water to wells. All the ground water in the area is derived from precipitation. It is estimated that about 5 percent of the precipitation infiltrates directly to the zone of saturation. The remainder either is evaporated immediately; is retained by the soil, later to be evaporated or transpired; or is discharged by overland flow to the surface drainage courses. Most of the water that reaches the surface drainage courses eventually sinks to the zone of saturation or is evaporated. The slope of the water table and the movement of ground water are generally eastward. The depth to water ranges from less than 10 feet in parts of the valley to about 300 feet in the upland areas. In much of the Pine Bluffs lowland, the depth to water is less than 50 feet. Ground water not pumped from wells within the area is discharged by evapotranspiration where the water table is close to the land surface, by outflow into streams, or by underflow eastward beneath the State line. \r\n\r\nThe chemical quality of ground water from the principal sources is remarkably uniform, and the range in concentration of dissolved constituents is narrow. In general, the water is of the calcium bicarbonate type, is hard (hardness as CaC03 is as high as 246 ppm), and contains less than about 400 parts per million of dissolved solids, which is a moderate mineralization. Silica constitutes a large proportion of the dissolved solids. \r\n\r\nThe water is suitable for irrigation and, except for iron in water from some wells that tap the Ogallala formation, meets the drinking water standards of the U.S. Public Health Service for chemical constituents. Because the water is siliceous, alkaline, and hard, it is unsuitable for many industrial uses unless treated.","language":"ENGLISH","publisher":"U.S. Govt. Print. 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